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- W2371102548 abstract "The Jiaojiang River Estuary is shallow, macro-tide dominated, highly turbid, and has large freshwater discharge variations. The mixing processes include phenomena such as freshwater front, salt wedge and vertical negative salinity gradient. This paper presents the analyzed result of the mixing processes in Jiaojiang River Estuary and the effects of both hydrodynamics and fine sediment dynmics using a set of observational field data collected in April, 1991.During spring tidal flood, the water column is verically homogenous, but has a freshwater front in the estuary. A lm thick fluid mud layer capped by a lutocline is formed when the tidal current velocity is less 0.3ms-1. The low-salinity water trapped in the fluid mud layer underlying more salty water enhances vertical mixing when the fluid mud layer is eroded.During the neap, two lutoclines exist in the water column for 80%-90% of observation time in two tidal cycles. The lutocline's contributions to the water column stability are 17 times larger than that of the maximum salinity gradient ever observed throughout our study. The water column is stratified due to the lutoclines and the high suspended sediment concentions inhibiting the vertical mixing. The freshwater front present in spring hde evolvedinto a salt wedge." @default.
- W2371102548 created "2016-06-24" @default.
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- W2371102548 date "1998-01-01" @default.
- W2371102548 modified "2023-09-23" @default.
- W2371102548 title "MIXING PROCESS IN HIGHLY TURBID WATERS OF JIAOJIANG RIVER ESTUARY" @default.
- W2371102548 hasPublicationYear "1998" @default.
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